Variation of Runoff and Influence of Human Activity Rate in Kuye River Basin

GUO Qiao-ling; CHEN Xin-hua; LIU Pei-wang; FANG Hai-jun

doi:10.13961/j.cnki.stbctb.2014.04.034

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Variation of Runoff and Influence of Human Activity Rate in Kuye River Basin

- Variation of Runoff and Influence of Human Activity Rate in Kuye River Basin
- Bulletin of Soiland Water Conservation Vol. 33, Issue 4, Pages: 110-113(2014)
- 作者机构：
  
  1. 河南理工大学资源环境学院,河南,焦作,454003
  2. 黄河中游水文水资源局, 山西榆次,030600
  3. 河南安宏信息科技有限公司,河南,郑州,450000
- 作者简介：
- 基金信息：
- DOI：10.13961/j.cnki.stbctb.2014.04.034
  CLC：
- Published：2014
- 稿件说明：
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GUO Qiao-ling, CHEN Xin-hua, LIU Pei-wang, et al. Variation of Runoff and Influence of Human Activity Rate in Kuye River Basin[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 110-113.
DOI：

GUO Qiao-ling, CHEN Xin-hua, LIU Pei-wang, et al. Variation of Runoff and Influence of Human Activity Rate in Kuye River Basin[J]. Bulletin of Soiland Water Conservation, 2014, 33(4): 110-113. DOI： 10.13961/j.cnki.stbctb.2014.04.034.

摘要

利用王道恒塔、温家川2个水文站的实测降水、径流资料

应用M-K秩相关系数、R/S分析、降水-径流双累积曲线法等多种数值模型方法

分析了窟野河径流年际变化特征、径流变化趋势、降水变化以及人类活动对径流变化的影响。结果表明:(1) 窟野河流域多年径流变化呈下降趋势

20世纪末以来尤为明显。(2) 王道恒塔和温家川2个水文站的Hurst指数分别为0.853和0.803

表明未来一段时间内窟野河年径流变化趋势将与过去保持同一势态

有持续递减的特征。(3) 不同历史阶段

人类活动的剧烈程度不同

对径流量减少的影响亦不同。影响最剧烈的阶段为1997-2010年

该阶段人类活动对径流减少的影响所占比例在2个水文站分别高达80.48%和93.62%。人类活动的加剧是导致窟野河径流量锐减的主要原因。

Abstract

Based on historical records from two hydrological stations of Wangdaohengta and Wenjiachuan

the runoff variation characteristics and influence factors

which include runoff inter-annual variation characteristics

changing trend

precipitation change

and the impact of human activities

were analyzed by using different analyzing methods

such as Mann-Kendall trend analysis

R/S analysis

and double mass curve for annual rainfall stream flow. The results showed that the multi-year change of runoff had a distinctive decreased tendency

especially since the end of the 20th Century. The Hurst index were 0.853 and 0.803 for the Wangdaohengta and Wenjiachuan stations

respectively

which indicates that the decreasing trends of runoff in Kuye River would continue in the future.The rainfall and human activities had a different influence on runoff in different periods. During 1997-2010

the runoff descending proportions caused by the human activities are as high as 80.48% and 93.62% in Wangdaohengta and Wenjiachuan stations

therefor aggravating human activities were the main reason for runoff descending in Kuye River.

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